Abstract

The use of Eh-pH diagrams in geochemistry is widespread, and their application to many aspects of mineral paragenesis well documented. These diagrams have been proven useful for metallurgical purposes, for predicting species in solutions, for alteration products of ores and in hydrothermal systems, and many others.

Keywords

Sulfide Geochemistry Calcite Radioactive Element Gypsum 

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Copyright information

© Springer-Verlag Berlin Heidelberg 1988

Authors and Affiliations

  • Douglas G. Brookins
    • 1
  1. 1.Department of GeologyUniversity of New MexicoAlbuquerqueUSA

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